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Morgan Upland
Morgan Upland () is a featureless undulating snow plateau in the central Antarctic Peninsula bounded by Cole Glacier and Clarke Glacier on the north and west, by Weyerhaeuser Glacier on the east, by Airy Glacier on the south, and Hariot Glacier on the southwest. The area was photographed from the air in September 1962 by the British Antarctic Survey The British Antarctic Survey (BAS) is the United Kingdom's national polar research institute. It has a dual purpose, to conduct polar science, enabling better understanding of global issues, and to provide an active presence in the Antarctic on ... (BAS) air unit, and the photos were used by BAS surveyor Ivor P. Morgan, for whom the upland is named, who compiled a map over the period 1961 to 1964. References Plateaus of Antarctica Landforms of Graham Land Fallières Coast Bowman Coast {{FallièresCoast-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Antarctic Peninsula
The Antarctic Peninsula, known as O'Higgins Land in Chile and Tierra de San Martín in Argentina, and originally as Graham Land in the United Kingdom and the Palmer Peninsula in the United States, is the northernmost part of mainland Antarctica. The Antarctic Peninsula is part of the larger peninsula of West Antarctica, protruding from a line between Cape Adams (Weddell Sea) and a point on the mainland south of the Eklund Islands. Beneath the ice sheet that covers it, the Antarctic Peninsula consists of a string of bedrock islands; these are separated by deep channels whose bottoms lie at depths considerably below current sea level. They are joined by a grounded ice sheet. Tierra del Fuego, the southernmost tip of South America, is about away across the Drake Passage. The Antarctic Peninsula is in area and 80% ice-covered. The marine ecosystem around the western continental shelf of the Antarctic Peninsula (WAP) has been subjected to rapid climate change. Over the past 50 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cole Glacier
Mobiloil Inlet () is an ice-filled inlet, nurtured by several northeast and east flowing glaciers, lying between the Rock Pile Peaks and Hollick-Kenyon Peninsula along the east coast of the Antarctic Peninsula. It was discovered by Sir Hubert Wilkins in a flight on December 20, 1928, and named by him after a product of the Vacuum Oil Company of Australia. Yates Spur, a prominent rock spur A spur is a metal tool designed to be worn in pairs on the heels of riding boots for the purpose of directing a horse or other animal to move forward or laterally while riding. It is usually used to refine the riding aids (commands) and to back ..., projects from the south side of the inlet. References Inlets of Graham Land Bowman Coast ExxonMobil {{BowmanCoast-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Clarke Glacier (Graham Land)
Clarke Glacier is a -wide, -long glacier, located on the west coast of Graham Land in Antarctica. It flows west, along the north side of Sickle Mountain and the Baudin Peaks, to Mikkelsen Bay. It was first surveyed in 1936 by the British Graham Land expedition (BGLE) (1934-1937) under John Rymill. In January 1941, it was traversed near its head by a United States Antarctic Service (USAS) sledge party. The lower reaches of the glacier were surveyed in 1948-1949 by the Falkland Islands Dependencies Survey (FIDS), who named the glacier (decision year 1955). The glacier was named for Louis C. G. Clarke, director of the Fitzwilliam Museum, Cambridge from 1937 to 1946, who "greatly assisted the BGLE." See also * List of glaciers in the Antarctic * Geography of Antarctica * Geology of Antarctica * Glaciology Glaciology (; ) is the scientific study of glaciers, or more generally ice and natural phenomena that involve ice. Glaciology is an interdisciplinary Earth science th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Weyerhaeuser Glacier
Weyerhaeuser Glacier () is a large glacier flowing north into Mercator Ice Piedmont close west of Mobiloil Inlet, on the east coast of Antarctic Peninsula. This glacier lies in the area first explored from the air by Sir Hubert Wilkins in 1928 and Lincoln Ellsworth in 1935, but it was first clearly delineated in aerial photographs taken by the United States Antarctic Service (USAS) in 1940. The glacier was resighted in 1947 by the Ronne Antarctic Research Expedition (RARE) under Ronne. He named it for F. K. Weyerhaeuser, of the Weyerhaeuser Timber Co., who contributed lumber and insulating material to the expedition. See also *Mount McAllister Mount McAllister () is a mountain rising to on the west side of Weyerhaeuser Glacier, northwest of Mount Blunt in the east of the Antarctic Peninsula. The peak was photographed from the air by the United States Antarctic Service, 1940, the Ron ..., rising to 1,975 metres (6,480 ft) on the west side of Weyerhaeuser Glacier Referen ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Airy Glacier
The Airy Glacier () is a glacier long and wide, flowing west to the northeast portion of Forster Ice Piedmont, near the west coast of the Antarctic Peninsula. The glacier was first roughly surveyed by British Graham Land Expedition of 1936–37, then photographed from the air by the Ronne Antarctic Research Expedition in 1947, and surveyed by Falkland Islands Dependencies Survey in 1958. It was named by United Kingdom Antarctic Place-Names Committee for George Biddell Airy, British Astronomer Royal, who in 1839 introduced a method of correcting magnetic compass A compass is a device that shows the cardinal directions used for navigation and geographic orientation. It commonly consists of a magnetized needle or other element, such as a compass card or compass rose, which can pivot to align itself with ...es for deviation. See also * List of glaciers in the Antarctic * Norman Peak References Glaciers of Palmer Land {{PalmerLand-glacier-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hariot Glacier
Hariot Glacier () is a glacier flowing northwest along the south side of Morgan Upland before turning west into the northern portion of the Wordie Ice Shelf, along the west coast of the Antarctic Peninsula. It was roughly surveyed by the British Graham Land Expedition, 1936–37, and the upper reaches were photographed from the air by the Ronne Antarctic Research Expedition, 1947. The glacier was surveyed from the ground by members of the Falkland Islands Dependencies Survey who travelled along it in December 1958, and it was named by the UK Antarctic Place-Names Committee after Thomas Hariot, an English mathematician who pioneered new methods of navigation under the patronage of Sir Walter Raleigh. References Glaciers of Fallières Coast {{FallièresCoast-glacier-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
British Antarctic Survey
The British Antarctic Survey (BAS) is the United Kingdom's national polar research institute. It has a dual purpose, to conduct polar science, enabling better understanding of global issues, and to provide an active presence in the Antarctic on behalf of the UK. It is part of the Natural Environment Research Council (NERC). With over 400 staff, BAS takes an active role in Antarctic affairs, operating five research stations, one ship and five aircraft in both polar regions, as well as addressing key global and regional issues. This involves joint research projects with over 40 UK universities and more than 120 national and international collaborations. Having taken shape from activities during World War II, it was known as the Falkland Islands Dependencies Survey until 1962. History Operation Tabarin was a small British expedition in 1943 to establish permanently occupied bases in the Antarctic. It was a joint undertaking by the Admiralty and the Colonial Office. At the end of t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ivor P
Ivor is an English masculine given name derived either directly from the Norse ''Ívarr'', or from Welsh (which spells it ''Ifor''), Irish (sometimes ''Ibar''), or Scottish, all of which likely derive it also from the original Norse form.The Oxford Dictionary of Christian Names (1947) by E. G. Withycombe The Norse name is derived from the Old Norse elements ''ýr'' (yew, bow) and ''herr'' (warrior, army): hence, 'archer, bow warrior'. It is possible the old Norse name ''Ívarr'' comes from the Celtic root and may be related to the Celtic root of ''-iv'' which is found in ''St. Ives'' for example, itself possibly referring to yew. This could indicate an earlier shared language origin; potentially through Indo-European, previous contact or another source. Some of the earliest known bearers of the name are Ibar of Beggerin, an Irish saint who may have preceded or been contemporary with St. Patrick and probably died in the 500s; Ivar the Boneless, an 800s Viking who was possibly identi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Plateaus Of Antarctica
In geology and physical geography, a plateau (; ; ), also called a high plain or a tableland, is an area of a highland consisting of flat terrain that is raised sharply above the surrounding area on at least one side. Often one or more sides have deep hills or escarpments. Plateaus can be formed by a number of processes, including upwelling of volcanic magma, extrusion of lava, and erosion by water and glaciers. Plateaus are classified according to their surrounding environment as intermontane, piedmont, or continental. A few plateaus may have a small flat top while others have wide ones. Formation Plateaus can be formed by a number of processes, including upwelling of volcanic magma, extrusion of lava, Plate tectonics movements and erosion by water and glaciers. Volcanic Volcanic plateaus are produced by volcanic activity. The Columbia Plateau in the north-western United States is an example. They may be formed by upwelling of volcanic magma or extrusion of lava. The un ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Landforms Of Graham Land
A landform is a natural or anthropogenic land feature on the solid surface of the Earth or other planetary body. Landforms together make up a given terrain, and their arrangement in the landscape is known as topography. Landforms include hills, mountains, canyons, and valleys, as well as shoreline features such as bays, peninsulas, and seas, including submerged features such as mid-ocean ridges, volcanoes, and the great ocean basins. Physical characteristics Landforms are categorized by characteristic physical attributes such as elevation, slope, orientation, stratification, rock exposure and soil type. Gross physical features or landforms include intuitive elements such as berms, mounds, hills, ridges, cliffs, valleys, rivers, peninsulas, volcanoes, and numerous other structural and size-scaled (e.g. ponds vs. lakes, hills vs. mountains) elements including various kinds of inland and oceanic waterbodies and sub-surface features. Mountains, hills, plateaux, and plains are the fo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fallières Coast
The Fallières Coast is that portion of the west coast of the Antarctic Peninsula between the head of Bourgeois Fjord and Cape Jeremy and lies on Marguerite Bay and the Wordie Ice Shelf. On the south it is joined by Rymill Coast, and in the north by Loubet Coast. Fallières Coast was first explored in January 1909 by the French Antarctic Expedition under J.B. Charcot, who named it for Armand Fallières, then President of France The president of France, officially the president of the French Republic (french: Président de la République française), is the executive head of state of France, and the commander-in-chief of the French Armed Forces. As the presidency i .... References Coasts of Graham Land {{FallièresCoast-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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